气候变化对埃塞俄比亚青尼罗流域Didessa流域水文和水资源有效性的潜在影响

Sintayehu Legesse Gebre, K. Tadele, B. G. Mariam
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引用次数: 40

摘要

这项研究是在位于青尼罗河流域西南部的迪迪萨流域进行的。这部分流域的地理位置非常重要,因为不同的水资源开发都在这里进行,比如大复兴大坝和其他开发项目,因此研究和评估气候变化对水文和水资源可用性的潜在影响至关重要。利用ECHAM5 (GCM) 50 km分辨率动态降尺度数据输出,建立了A1B排放情景下2030年(2031-2040年)和2090年(2091-2100年)降水、温度和潜在蒸发量的未来气候变化情景。与基线期(1991-2000年)相比,GCM气候变量模式的未来预估显示出增加的趋势。2030年和2090年,Didessa流域的年平均降水量可能分别增加+33.22%和+8.40%。将气候变化变量作为HBV水文模型的输入,模拟了Arjo镇附近测量站未来径流。气候变化对流域未来径流量的影响导致流域出水口平均径流量呈正数量级变化。平均径流量的增加与流域降水预测的增加有关。在夏季主要雨季,2030年和2090年的平均季节径流百分比变化可能分别比基线期增加+157%和+136%。因此,未来更有可能的是,集水区的水资源可用性可能会增加。这可能为小规模农民创造机会,在雨季利用足够的水供以后使用。
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Potential Impacts of Climate Change on the Hydrology and Water resources Availability of Didessa Catchment, Blue Nile River Basin, Ethiopia
This study was carried out in Didessa catchment, which is situated in the south-west part of Blue Nile River Basin. This part of the basin is very important due to the location of the place where different water resources development are undertaking, like the Grand Renaissance dam and other development projects, So it was crucial to study and evaluate the potential impacts of climate change on the hydrology and water resources availability. Future Climate change scenarios of precipitation, temperature and potential evaporation were developed using output of dynamically downscaled data of ECHAM5 (GCM) 50 Kms resolution under A1B emission scenario for 2030’s (2031-2040) and 2090’s (2091-2100). The future projection of the GCM model of climate variables showed an increasing trend as compared to the base line period (1991-2000). At 2030`s and 2090`s average annual precipitation may increases by +33.22% and+8.40% respectively over the Didessa catchment. The climate changes variables used as input in to HBV hydrological model to simulate the future runoff at the out let of gauging station of Near Arjo town. The impact of climate change on future runoff resulted a positive magnitude change in average runoff flow at the outlet of the catchment. The increase in average runoff is associated with the increase in precipitation projection over the catchment. During the main rainy season of summer, at 2030`s and 2090`s average seasonal runoff percentage change may increase up to+157% and+136% respectively as compared to the base line period. Hence, more likely in the future the water resources availability may increases in the catchment. This may create an opportunity for small scale farmers to harness enough amount of water during rainy season for later use.
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